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  • Oct 20, 2026, 6:28 PM

    Capital investment in decades of painstaking research richly pays off by making a model possible:

    ''We find that slow bedrock adjustment weakens the stabilizing effect of glacial isostatic adjustment, allowing grounding lines to reach retrograde bed slopes more readily and triggering self-sustained retreat below the bifurcation threshold. Although the West Antarctic Ice Sheet is subject to a bifurcation, it is unlikely to experience rate-induced tipping because of the low mantle viscosity beneath the region. In contrast, the Recovery and Aurora subglacial basins are likely to undergo such a transition even under warming rates lower than those observed today.''

    #cryosphere
    #ClimateChange
    #isostasy

    nature.com/articles/s41561-026

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